The main geological provinces and boundaries of Greenland. The Rinkian fold–thrust belt is a broad belt of deformation in the Rae craton that formed the lower plate of the Nagssugtoqidian suture. Tectonic subdivisions and boundaries within the Rinkian fold–thrust belt are uncertain although many of the major elements of the geology including the Palaeoproterozoic sedimentary cover sequences and the Prøven igneous complex (part of the Cumberland batholith) are present also on Baffin Island. PIC, Prøven Igneous Complex; KF, Karrat Fjord; UF, Uummannaq Fjord; M, Maarmorilik; AN, Anap Nuna; DB, Disko Bugt; SF, Søndre Strømfjord. Modified from St.-Onge et al. (2009). Printed with permission from Geological Society, London.
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